The different bands in sedimentary formations are called strata.
Rocks can show changes through processes like sedimentation, metamorphism, and weathering. The presence of different types of rocks, such as sedimentary, igneous, and metamorphic, can indicate past environmental conditions and overall geological change over time. Fossils found in rocks can also demonstrate biological changes that have occurred.
Weatheing is where rocks and materials are broken down by the weather an uplifting is literally lifting up of land!
Weathering, erosion, and biological activity are processes that break down rocks and other materials at Earth's surface. These processes collectively contribute to the breakdown and decomposition of rocks through physical, chemical, and biological means. Weathering can be caused by factors such as water, wind, temperature changes, and plant roots, leading to the disintegration and decomposition of rocks over time.
Rock changes involve physical or chemical processes that transform rocks into different forms, but they do not destroy or create matter. These changes are part of the rock cycle, where rocks are constantly being formed, broken down, and reformed. The principle of conservation of matter states that matter is neither created nor destroyed in these processes.
Because they are made of different materials
weathering
Physical weathering is due to: rocks hitting other rocks causing them to break up from the action of frost and ice the action of wind or waves or running water the action of plants. Chemical weathering changes the composition of the rock and is due to: water dissolving minerals in the rock oxidation of metals in the rock
The four different types of chemical weathering are hydration, oxidation, carbonic acid action and hydrolysis. Chemical weathering is a chemical reaction that erodes certain things such as building materials and rocks.
The main types of rocks that form from the deposition of different materials on Earth are sedimentary rocks. These rocks are created from the accumulation and compression of sediments, such as sand, silt, and clay, typically through processes like erosion and deposition. Examples of sedimentary rocks include sandstone, shale, and limestone.
They are could consist of different materials, like clay, sand, or rocks.
Weathering and erosion of the weather materials, their transport and deposition as new sediments.
Yes. Temperature changes, water, wind, pressure changes, plant and animal action, and gravity are all agents of physical weathing.
Igneous, sedimentary, and metamorphic rocks are the three main types of rocks. Igneous rocks form from the cooling and solidification of magma or lava. Sedimentary rocks are formed through the accumulation and cementation of sediments. Metamorphic rocks are rocks that have undergone significant physical or chemical changes due to heat and pressure.
it is the materials on the periodic table and rocks such as ignous rocks sedimentry and metamorphic rocks and many many more!
The different bands in sedimentary formations are called strata.
Parent rocks of metamorphic rocks can include igneous, sedimentary, or pre-existing metamorphic rocks. These rocks undergo changes in mineralogy and texture due to heat, pressure, and chemical processes without melting, resulting in the formation of metamorphic rocks. Different parent rocks can give rise to different types of metamorphic rocks.